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Filters: Tags: McKinley County, New Mexico (X) > partyWithName: Sears, J.D. (X)

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Hosta sandstone member of Mesaverde formation, showing mode of weathering of upper part: view in sec. 4, T. 17 N., R. 16 W. McKinley County, New Mexico. 1930. Plate 31-C. U.S.Geological Survey Professional paper 193. 1941.
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Hosta sandstone member of Mesaverde formation split by Satan tongue of Mancos shale; upper two ledges of sandstone are the Hosta; intervening shale is the Satan tongue; intermediate slope, lower part of Gibson coal member; sandstones in foreground, the Dalton sandstone member, view looking west at north end of Satan Pass, southeast of Crown Point. McKinley County, New Mexico. 1930. Plate 28-C, U.S.Geological Survey Professional paper 193. 1941.
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Transition zone marking contact between Mulatto tongue of Mancos shale and overlying Dalton sandstone member of Mesaverde formation: view on east side of Satan Pass in sec. 20, T. 16 N., R. 12 W. McKinley County, New Mexico. 1930. Plate 31-B. U.S.Geological Survey Professional paper 193. 1941
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Intertonguing of Ostrea soleniscus marl with layers of the "Stray sandstone". The marl is composed largely of Ostrea soleniscus: The bed sandstone contains only scattered remains of the elongated oyster. View in sec. 9, T.14 N., R.9 W. Photo by, J.D. Sears. McKinley County, New Mexico. 1930. Plate 30-C U.S.Geological Survey Professional paper 193-F. 1941.
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Upper part of Mancos shale and basal sandstones of Mesaverde formation, near north end of the hogback north of Gallup, the top of the Gryphaea newberryi zone is at the right. This is photo 157 and 158 composed as one. McKinley County, New Mexico. 1930. Plate 27-A, U.S.Geological Survey Professional paper 193. 1941.
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Gibson coal member of Mesaverde formation west of (landward from) area in which it is split by the Hosta sandstone member; view in T.17 N., R. 17 W. McKinley County, New Mexico. 1929. Plate 29-C, U.S.Geological Survey Professional paper 193. 1941.
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Sandy marl composed largely of Ostrea solenis, the indicated specimen is 18 inches long. Photo by, J.D. Sears. McKinley County, New Mexico. 1930. Plate 30-A, U.S.Geological Survey Professional paper 193-F. 1941. Album: T.14 N., R 9W., sec. 9. Ostrea soleniscus 18 inches long in boulder of "stray" sandstone.
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Closer view of the outcrop shown in photo 10: Photo by, J.D. Sears. McKinley County, New Mexico. 1930. Plate 30-B, U.S.Geological Survey Professional paper 193-F. 1941. Index Card: Near view of oyster reef shown in No. 10 From Album: T. 14 N., R. 9 W., sec. 9
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Mulatto tongue of Mancos shale overlain by Dalton sandstone member of Mesaverde formation, in foreground, the top of the "Stray sandstone". View in sec. 30, T. 15 N., R. 10 W. At this locality the Mulatto is about 250 feet thick. Through the combined effects of topographic slope, dip of beds, and foreshortening, the photograph greatly exaggerates the apparent thickness of the lower, rather sandy portion of the Mulatto, which extends as far up the tree covered bench at the left, as contrasted with the partly hidden upper, less sandy portion of the Mulatto. McKinley County, New Mexico. 1930. Plate 28-A, U.S.Geological Survey Professional paper 193. 1941.
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Gallup sandstone member of Mesaverde formation, showing mode of weathering: sec. 16, T. 14 N., R. 9 W. Photo by, J.D. Sears. McKinley County, New Mexico. 1930. Plate 29-A, U.S.Geological Survey Professional paper 193-F. 1941. Album: T. 14 N., R. 9W, Sec. 16: A sink hole in the Mancos Shale. Typical Gallup sandstone in back.
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Intertonguing of Mancos shale and Gallup sandstone member of Mesaverde formation. Foreground and lower slope, main body of Mancos; bench a sandstone wedge from the Gallup, thinning eastward (toward the right); upper slope, a tongue of Mancos thinning westwards; cliff, main body of Gallup sandstone member. McKinley County, New Mexico. 1930. A small portion of photo 154 (left) and all of photo 155 is plate 28-B, U.S.Geological Survey Professional paper 193. 1941.


    map background search result map search result map Intertonguing of Ostrea soleniscus marl with layers of the "Stray sandstone". McKinley County, New Mexico. 1930. Closer view of the outcrop shown in photo 10:  McKinley County, New Mexico. 1930 Sandy marl composed largely of Ostrea solenis, the indicated specimen is 18 inches long. McKinley County, New Mexico. 1930. Gallup sandstone member of Mesaverde formation, showing mode of weathering.  McKinley County, New Mexico. 1930. Intertonguing of Mancos shale and Gallup sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Upper part of Mancos shale and basal sandstones of Mesaverde formation. McKinley County, New Mexico. 1930. Gibson coal member of Mesa Verde formation. McKinley County, New Mexico. 1929. Hosta sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Hosta sandstone member of Mesaverde formation split by Satan tongue of Mancos shale. McKinley County, New Mexico. 1930. Mulatto tongue of Mancos shale overlain by Dalton sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Transition zone marking contact between Mulatto tongue of Mancos shale and overlying Dalton sandstone. McKinley County, New Mexico. 1930. Intertonguing of Ostrea soleniscus marl with layers of the "Stray sandstone". McKinley County, New Mexico. 1930. Closer view of the outcrop shown in photo 10:  McKinley County, New Mexico. 1930 Sandy marl composed largely of Ostrea solenis, the indicated specimen is 18 inches long. McKinley County, New Mexico. 1930. Gallup sandstone member of Mesaverde formation, showing mode of weathering.  McKinley County, New Mexico. 1930. Intertonguing of Mancos shale and Gallup sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Upper part of Mancos shale and basal sandstones of Mesaverde formation. McKinley County, New Mexico. 1930. Gibson coal member of Mesa Verde formation. McKinley County, New Mexico. 1929. Hosta sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Hosta sandstone member of Mesaverde formation split by Satan tongue of Mancos shale. McKinley County, New Mexico. 1930. Mulatto tongue of Mancos shale overlain by Dalton sandstone member of Mesaverde formation. McKinley County, New Mexico. 1930. Transition zone marking contact between Mulatto tongue of Mancos shale and overlying Dalton sandstone. McKinley County, New Mexico. 1930.